Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Over the past couple of weeks, several large avalanches have failed on faceted weak layers deeper in the snowpack. These include a natural avalanche on Carbonate Hil, a remotely triggered avalanche on Mt. Emmons on Sunday, and several human-triggered slides the previous week (Hunter Hill, Snowmass). Persistent slab activity has been infrequent this month and most problematic on wind-loaded terrain. Last week's loading event produced surprisingly little avalanche activity and adds to the infrequent characterization of this avalanche problem recently.
At below treeline elevations, there are some areas in the SE Mountains that have seen a foot of snow accumulate on a weak old snow surface. In general, the slabs above that weak snow remain soft and may not be enough to propagate a slab avalanche. In open areas at these lower elevations past winds will have stiffened those slabs or created thicker slabs in some areas that will be more reactive to human triggering. If you are riding steep below treeline slopes, keep an eye on these slab/weak layer characteristics.
2/23: A surprising collapse that broke around 3 feet deep into the snowpack on northeast-facing terrain on Mount Emmons.